Water deposits the clay particles in thin, flat layers.
You could say it had plane cleavages. What happens is that bonds between the molecular planes are much weaker than those in the plane of the cleavage. Graphite and mica would be good examples.
Mos flat rocks are sedimentary, with shale being a prime example. Shale forms from fine sediment being laid down in layers and then later hardened into rock, with the layers preserved. Slate is a metamorphic rock derived from shale that still preserves the layering.
The cleavage properties of mica result from its layered structure, where weak van der Waals forces hold the layers together. This allows the mineral to easily split along these planes, producing smooth, flat surfaces. The perfect cleavage in one direction is characteristic of mica, enabling it to be easily separated into thin sheets. This unique property makes mica valuable in various applications, including electronics and cosmetics.
A mineral's ability to split easily along planes of weakness, producing flat surfaces.
it probably break apart with cleavage, because the carbon atoms in graphite from sheets that could split apart easily in layers.
Sedimentary rock, such as sandstone or shale, often has visible flat layers called strata that form from the accumulation and compression of sediments over time. These layers can be easily distinguished in sedimentary rocks due to their distinct horizontal orientation.
graphite breaks by cleavage because the bonds between its atoms are less strong in directions
Sedimentary rocks have flat layers.
Stratus is the cloud in flat layers
Cleavage. Slate exhibits excellent cleavage due to the alignment of its minerals in flat layers, allowing it to split easily along these planes. This property makes slate a popular choice for roofing tiles and other construction uses.
Slate is a fine-grained gray, green, or blue metamorphic rock that is easily flattened. The splitting of slate into flat layers illustrates its foliation.
The mineral that is flat with flaky cleavage is mica. Mica is a group of silicate minerals that can easily be split into thin sheets or flakes. These sheets have excellent cleavage, making them easily separable into thin layers.
Clouds in flat layers are called stratus.
Graphite will break apart with cleavage because the carbon atoms are arranged in layers that have weak bonds between them. This allows the layers to slide past each other easily, resulting in cleavage along flat planes.
The type of rock that breaks apart into flat planar sections is called a sedimentary rock, specifically those that exhibit layering, such as shale. Shale is composed of fine particles and clay minerals that align in such a way that it can split easily along these layers. This characteristic is due to the processes of sedimentation and compaction, which create distinct planes of weakness in the rock. Other types of rocks, like schist or gneiss, also exhibit foliation and can break in flat sections but are metamorphic in nature.
slateschist